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20 SOCIETY OF VERTEBRATE PALEONTOLOGY, MEMOIR 3<br />
culature is very clear (BMNH R11956, R8501, RUB 17), passing<br />
through a canal formed by maxilla, lacrimal, jugal, and<br />
perhaps palatine. The maxilla and lacrimal (BMNH R11956)<br />
are both strongly grooved for the neurovascular bundle. In fact,<br />
the dorsal groove on the maxilla extends rostrally within the<br />
floor <strong>of</strong> the antorbital cavity, ending at a slit-like foramen directed<br />
ventrally into the bone and opposite the internal antorbital<br />
fenestra (BMNH R11956). This slit almost certainly conducted<br />
the maxillary neurovasculature because all <strong>of</strong> the external<br />
neurovascular foramina are directed toward it (Fig. 7A).<br />
Among Ornithopoda, as in Lesothosaurus diagnosticus, Heterodontosaurus<br />
tucki (BMNH R8 179 [cast <strong>of</strong> SAM 3371) probably<br />
had a neurovascular canal between maxilla, lacrimal, and<br />
jugal. However, more similar to Hypsilophodon foxii (discussed<br />
below), the neurovascular branches exited more or less separately<br />
from the antorbital cavity rather than from a single foramen.<br />
Better data are available for Hypsilophodon foxii<br />
(BMNH R197, R192, R5862, R2477). The dorsal surface <strong>of</strong> the<br />
palatine (BMNH R2477) has a clear fossa extending rostrally<br />
up to the choana (Fig. 8A). Unlike Lesothosaurus diagnosticus,<br />
there is no nasal fossa rostral to it, but the postchoanal strut is<br />
grooved dorsally for the nasal capsule. As in L. diagnosticus,<br />
however, there is a very clear neurovascular canal formed by<br />
maxilla, jugal, lacrimal, and a dorsal, laterally arching process<br />
<strong>of</strong> the palatine (Fig. 8A). The portion <strong>of</strong> the maxilla forming<br />
the ventral rim <strong>of</strong> the external antorbital fenestra (supralveolar<br />
lamina) is drawn up dorsally such that the nerves and vessels<br />
would be lodged in a deep groove. As alluded to above, the<br />
neurovasculature exited the antorbital cavity ventrolaterally via<br />
several large foramina (Fig. 8B).<br />
Whereas these more basal ornithopods retain the basic crani<strong>of</strong>acial<br />
architecture <strong>of</strong> other archosaurs, the facial and palatal<br />
skeleton in iguanodontian ornithopods becomes highly-transformed.<br />
with reduction <strong>of</strong> the antorbital cavity and development<br />
<strong>of</strong> larger dentitions (Weishampel, 1984; se; section on trends<br />
below). Probably above the level <strong>of</strong> Iguanodon spp. within Iguanodontia,<br />
the palatine assumes a much more vertical orientation<br />
(Fig. 11A; Lambe, 1920; Heaton, 1972; Norman, 1980;<br />
Norman and Weishampel, 1990; Weishampel and Horner,<br />
1990), largely occluding the postnasal fenestra and restricting<br />
the rostral advance <strong>of</strong> any pterygoideus musculature. The more<br />
basal iguanodontians retaining an antorbital cavity, such as<br />
Camptosaurus dispar (UUVP 5946), C. prestwichii (Galton and<br />
Powell, 1980), and Iguanodon ather-eldensis (BMNH R5764,<br />
R11521), nevertheless resemble more basal ornithischians with<br />
regard to the relationship <strong>of</strong> the neurovasculature. There is a<br />
deep groove in the dorsal surface <strong>of</strong> the maxilla which is<br />
formed into a canal by the addition <strong>of</strong> the jugal and palatine<br />
(the jugal excludes the lacrimal from the canal in at least Iguanodon<br />
atherfieldensis; Fig. 11B). This groove extends in the floor<br />
<strong>of</strong> the small antorbital cavity before entering the neurovascular<br />
foramen located opposite the antorbital fenestra (as in Lesothosaurus<br />
diagnosticus; see Fig. 1lB for Iguanodon ather-eldensis).<br />
Hadrosaurs have a completely closed external antorbital<br />
fenestra (Weishampel and Horner, 1990), yet retain a shallow<br />
fossa on the palatine and the same basic structure <strong>of</strong> the neurovascular<br />
canal (e.g., Edmontosaurus regalis, CMN 2289;<br />
Corythosaurus casuarius, AMNH 5338; Hypacrosaurus sp.,<br />
MOR-609-88-9 I)<br />
The evidence provided by the basal thyreophoran Scelidosaurus<br />
harrisonii (BMNH R1111) is particularly important because<br />
many higher thyreophorans are so derived that direct correspondences<br />
are difficult to identify. S. harrisonii resembles<br />
Hypsilophodon foxii in that the caudodorsal surface <strong>of</strong> the palatine<br />
is excavated into a fossa extending up to the choana and<br />
the postchoanal strut is grooved for the nasal cartilages. Likewise,<br />
very similar to the other ornithischians discussed here,<br />
there is a neurovascular canal formed by maxilla, lacrimal, ju-<br />
gal, and palatine that is carried rostrally as a groove in the floor<br />
<strong>of</strong> the antorbital cavity, entering the body <strong>of</strong> the maxilla at a<br />
foramen opposite the antorbital fenestra. Emausaurus ernsti<br />
(Haubold, 1990) is an even more basal thyreophoran, retaining<br />
a much larger antorbital cavity. Although the existence <strong>of</strong> a<br />
muscular fossa on the palate is unknown, the course <strong>of</strong> the<br />
maxillary neurovasculature in E. ernsti closely resembles that<br />
in Scelidosaurus harrisonii and other ornithischians.<br />
The basal ceratopsian Psittacosaurus mongoliensis (AMNH<br />
6535; see Sereno, 1987) holds similar importance as a more<br />
basal member <strong>of</strong> a very specialized group. It also has a shallow<br />
fossa on the dorsolateral surfaces <strong>of</strong> the palatine and pterygoid<br />
extending rostrally to the choanal margin and a neurovascular<br />
canal surrounded by maxilla, palatine, and jugal. The neurovascular<br />
canal is large and leads to a series <strong>of</strong> ventral foramina<br />
opening into the buccal cavity.<br />
Saurischians differ in that the maxillary neurovasculature is<br />
not typically enclosed in a canal formed by several bones; a<br />
canal is presumably an ornithischian apomorphy associated<br />
with the tendency to wall in the antorbital cavity (see section<br />
on trends below). Otherwise, some saurischians, such as Plateosaurus<br />
engelhardti, resemble such ornithischians as Lesothosaurus<br />
diagnosticus and Hypsilophodon foxii in the osteological<br />
correlates <strong>of</strong> the dorsal pterygoideus and maxillary neurovasculature.<br />
Most basal prosauropods (e.g., Thecodontosaurus<br />
antiquus, Kermack, 1984; Anchisaurus polyzelus, Galton, 1976)<br />
are poorly known with regard to the relevant features and the<br />
following discussion focuses mostly on Plateosaurus engelhardti<br />
(principally AMNH 6810; see also Galton, 1984, 1985c,<br />
1990). The dorsolateral surface <strong>of</strong> the palatine <strong>of</strong> P. engelhardti<br />
has a postchoanal strut that is strong laterally and weakens rostrodorsally,<br />
delimiting a caudal (muscular) fossa from a flatter,<br />
rostral, nasal area (Fig. 12D). Although Galton (1985~) did not<br />
list the palatine as an attachment site for the dorsal pterygoideus<br />
in P. engelhardti, the fossa compares well with the presumptive<br />
muscular fossa <strong>of</strong> other archosaurs.<br />
As in ornithischians, there is, within the antorbital cavity, a<br />
dorsal groove on the maxilla that passes rostrally until it enters<br />
a ventral, slit-like foramen opposite the rostral margin <strong>of</strong> the<br />
internal antorbital fenestra (Fig. 12D); as in Lesothosaurus<br />
diagnosticus, the external neurovascular foramina are all directed<br />
toward this slit (Fig. 12A). The dorsal groove and foramen<br />
apparently are present in Sellosaurus gracilis (Galton,<br />
1985b), and almost identical relationships <strong>of</strong> the external neurovascular<br />
foramina also are seen in that taxon and Massospondylus<br />
carinatus (Gow et al., 1990). Caudally in Plateosaurus<br />
engelhardti, processes <strong>of</strong> the lacrimal and palatine approach<br />
each other in the vicinity <strong>of</strong> their junction with the maxilla and<br />
jugal (Fig. 12D), but do not form the complete bony canal observed<br />
in the ornithischians (although it was probably completed<br />
with s<strong>of</strong>t tissue).<br />
As a whole, sauropods are poorly known with regard to these<br />
features. The palatines and pterygoids <strong>of</strong> Camarasaurus lentus<br />
(CM 11338; see also Madsen et al., 1995) and Diplodocus longus<br />
(CM 11161) are more or less vertically oriented in the<br />
vicinity <strong>of</strong> the antorbital cavity, with perhaps a slight concavity<br />
to their caudodorsolateral surfaces (Fig. 13A). The palatine <strong>of</strong><br />
Euhelopus zdanskyi has a stronger dorsolateral fossa, undercutting<br />
the postchoanal portion <strong>of</strong> the bone (Mateer and McIntosh,<br />
1985). Zhang's (1988) reconstruction <strong>of</strong> the adductor musculature<br />
attaching to this portion <strong>of</strong> the palate in Shunosaurus lii<br />
seems reasonable, although he carried the muscle rostrally onto<br />
the vomer which is unlikely. Janensch (1935-36) reconstructed<br />
the pterygoideus musculature <strong>of</strong> Brachiosaurus brancai as extending<br />
over the entire dorsal surface <strong>of</strong> the palatine to attach<br />
to the antorbital fenestra; however, the palatine <strong>of</strong> this form<br />
resembles that <strong>of</strong> Camarasaurus lentus (McIntosh, 1990; Mad-